Silicate minerals as a direct source of limiting nutrients: Siderophore synthesis and uptake promote ferric iron bioavailability from olivine and microbial growth-Reference-Cited by-同舟云学术

Silicate minerals as a direct source of limiting nutrients: Siderophore synthesis and uptake promote ferric iron bioavailability from olivine and microbial growth

Published:2021-06-09 Issue:6 Volume:19 Page:618-630
ISSN:1472-4677
Container-title:Geobiology
language:en
Short-container-title:Geobiology

Author:

Van Den Berghe Martin¹^ORCID,Merino Nancy¹²³,Nealson Kenneth H.¹,West A. Joshua¹

Affiliation:

1. Department of Earth Sciences University of Southern California Los Angeles CA USA

2. Earth‐Life Science Institute Tokyo Institute of Technology Tokyo Japan

3. Biosciences and Biotechnology division, Physical and Life Sciences Directorate Lawrence Livermore National Laboratory Livermore CA USA

Funder

National Aeronautics and Space Administration

John Templeton Foundation

Publisher

Wiley

Subject

General Earth and Planetary Sciences,General Environmental Science,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/gbi.12457

Reference108 articles.

1. Microbe–mineral interactions: The impact of surface attachment on mineral weathering and element selectivity by microorganisms

2. Iron transport in the genus Marinobacter

3. Siderophore-mediated iron uptake in two clades of Marinobacter spp. associated with phytoplankton: the role of light

4. Photolysis of iron-siderophore chelates promotes bacterial-algal mutualism

5. Geomorphology

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